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Soil Erosion Investigation Using Innovative Monitoring and Advanced Modelling

A special issue of Applied Sciences (ISSN 2076-3417). This special issue belongs to the section "Environmental Sciences".

Deadline for manuscript submissions: closed (31 August 2021) | Viewed by 11180

Special Issue Editor


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Guest Editor
Department of Aquatic Ecosystems Analysis and Management, Helmholtz Centre for Environmental Research-UFZ, Brückstrasse 3a, 39114 Magdeburg, Germany
Interests: soil erosion; sediment transport; catchment water quality; biogeochemistry; regional water quality assessment

Special Issue Information

Dear Colleagues,

Soil erosion is a severe environmental problem. Sediment derived from the soil represents an important threat to aquatic ecosystems by reducing light penetration and carrying pollutants such as pesticides and phosphorus, which physically damage freshwater. Physical understanding of soil erosion and sediment transport processes at various temporal and spatial scales and their controlling factors is crucial to better develop predictive tools. Further, obtaining quantitative information on soil redistribution patterns during storms events and their sediment sources are essential to develop effective management strategies and soil erosion mitigation measures at the catchment scale. This Special Issue encourages contributions on the understanding of soil erosion processes and sediment transport management based on detailed field works, laboratory experiments, validated numerical models, and effectiveness assessment methods. Investigation on high-frequency monitoring, sediment tracing, and fingerprinting techniques in association with other methods (including soil erosion modeling and sediment budgeting) are welcome.

Dr. Seifeddine Jomaa
Guest Editor

Manuscript Submission Information

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Keywords

  • soil erosion
  • sediment transport
  • monitoring
  • modeling
  • laboratory experiment
  • sediment source tracing
  • management strategies

Published Papers (4 papers)

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20 pages, 35009 KiB  
Article
Soil Erosion Estimates in Arid Region: A Case Study of the Koutine Catchment, Southeastern Tunisia
by Mongi Ben Zaied, Seifeddine Jomaa and Mohamed Ouessar
Appl. Sci. 2021, 11(15), 6763; https://doi.org/10.3390/app11156763 - 23 Jul 2021
Cited by 7 | Viewed by 3140
Abstract
Soil erosion remains one of the principal environmental problems in arid regions. This study aims to assess and quantify the variability of soil erosion in the Koutine catchment using the RUSLE (Revised Universal Soil Loss Equation) model. The Koutine catchment is located in [...] Read more.
Soil erosion remains one of the principal environmental problems in arid regions. This study aims to assess and quantify the variability of soil erosion in the Koutine catchment using the RUSLE (Revised Universal Soil Loss Equation) model. The Koutine catchment is located in an arid area in southeastern Tunisia and is characterized by an annual mean precipitation of less than 200 mm. The model was used to examine the influence of topography, extreme rainstorm intensity and soil texture on soil loss. The data used for model validation were obtained from field measurements by monitoring deposited sediment in settlement basins of 25 cisterns (a traditional water harvesting and storage technique) over 4 years, from 2015 to 2018. Results showed that slope is the most controlling factor of soil loss. The average annual soil loss in monitoring sites varies between 0.01 and 12.5 t/ha/y. The storm events inducing the largest soil losses occurred in the upstream part of the Koutine catchment with a maximum value of 7.3 t/ha per event. Soil erosion is highly affected by initial and preceding soil conditions. The RUSLE model reasonably reproduced (R2 = 0.81) the spatiotemporal variability of measured soil losses in the study catchment during the observation period. This study revealed the importance of using the cisterns in the data-scarce dry areas as a substitute for the classic soil erosion monitoring fields. Besides, combining modeling of outputs and field measurements could improve our physical understanding of soil erosion processes and their controlling factors in an arid catchment. The study results are beneficial for decision-makers to evaluate the existing soil conservation and water management plans, which can be further adjusted using appropriate soil erosion mitigation options based on scientific evidence. Full article
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14 pages, 2241 KiB  
Article
The Influence of Wave Nonlinearity on Cross-Shore Sediment Transport in Coastal Zone: Experimental Investigations
by Yana Saprykina
Appl. Sci. 2020, 10(12), 4087; https://doi.org/10.3390/app10124087 - 13 Jun 2020
Cited by 9 | Viewed by 2114
Abstract
On the basis of field experiment data, the main features of influence of non-linear wave transformation scenarios on cross-shore sediment transport in coastal zones were investigated. The bottom deformations due to the non-linear wave transformation follow the specific scenario. The increase in the [...] Read more.
On the basis of field experiment data, the main features of influence of non-linear wave transformation scenarios on cross-shore sediment transport in coastal zones were investigated. The bottom deformations due to the non-linear wave transformation follow the specific scenario. The increase in the second non-linear harmonic amplitude leads to the erosion of the underwater slope at the distances corresponding to this process, with the subsequent accumulation of sandy material closer to the shore at distances where the amplitude decreases during the backward energy transfer to the first harmonic. This can be explained by the change in the phase shift between harmonics during non-linear wave transformation. The second harmonic maximum provides the point near which the bottom deformations occur in different directions. Scenarios of non-linear wave transformation in which backward energy transfer from the second non-linear harmonic to the first is close to the shoreline will contribute to the transport and accumulation of the sediment on the coast. These scenarios are more characteristic of “small waves”. The scenario without a periodical exchange of wave energy between non-linear harmonics (with an increase in the second harmonic only) that is characteristic of large storm waves and plunging breaking waves will lead to the erosion of the underwater bottom profile. Full article
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14 pages, 6578 KiB  
Article
Estimating Non-Sustainable Soil Erosion Rates in the Tierra de Barros Vineyards (Extremadura, Spain) Using an ISUM Update
by Jesús Rodrigo-Comino, Jesús Barrena-González, Manuel Pulido-Fernández and Artemi Cerdá
Appl. Sci. 2019, 9(16), 3317; https://doi.org/10.3390/app9163317 - 13 Aug 2019
Cited by 10 | Viewed by 3225
Abstract
Monitoring soil erosion processes and measuring soil and water yields allow supplying key information to achieve land degradation neutrality challenges. Vineyards are one of the most affected agricultural territories by soil erosion due to human and natural factors. However, the spatial variability of [...] Read more.
Monitoring soil erosion processes and measuring soil and water yields allow supplying key information to achieve land degradation neutrality challenges. Vineyards are one of the most affected agricultural territories by soil erosion due to human and natural factors. However, the spatial variability of soil erosion, the number of sampling points, and plot size necessary to estimate accurate soil erosion rates remains unclear. In this research, we determine how many inter-rows should be surveyed to estimate the soil mobilization rates in the viticulture area of Tierra de Barros (Extremadura, SW Spain) using the Improved Stock Unearthing Method (ISUM). This method uses the graft union of the vines as a passive biomarker of the soil surface level changes since the time of plantation and inter-row measures. ISUM was applied to three inter-row and four rows of vines (5904 sampling points) in order to determine how many surfaces and transects must be surveyed as all the previous surveys were done with only one inter-row. The results showed average values of soil depletion reaching −11.4, −11.8, and −11.5 cm for the inter-rows 1, 2, and 3, respectively. The current soil surface level descended 11.6 cm in 20 years. The inter-rows 1, 2, and 3 with a total area of 302.4 m2 each one (2016 points) recorded 71.4, 70.8, and 74.0 Mg ha−1 yr−1, respectively. With the maximum number of sampling points (5904), 71.2 Mg ha−1 yr−1 were obtained. The spatial variability of the soil erosion was shown to be very small, with no statistically significant differences among inter-rows. This could be due to the effect of the soil profile homogenization as a consequence of the intense tillage. This research shows the potential predictability of ISUM in order to give an overall overview of the soil erosion process for vineyards that follow the same soil management system. We conclude that measuring one inter-row is enough to get an overview of soil erosion processes in vineyards when the vines are under the same intense tillage management and topographical conditions. Moreover, we demonstrated the high erosion rates in a vineyard within the viticultural region of the Tierra de Barros, which could be representative for similar vineyards with similar topographical conditions, soil properties, and a possible non-sustainable soil management system. Full article
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10 pages, 3775 KiB  
Technical Note
Visualization of the Onset of Scour under a Pipeline in Waves
by Yehui Zhu, Liquan Xie, Tsun-Ming Wong and Tsung-Chow Su
Appl. Sci. 2020, 10(9), 2994; https://doi.org/10.3390/app10092994 - 25 Apr 2020
Cited by 3 | Viewed by 1926
Abstract
This paper visualizes the onset of scour under a pipeline in regular waves and studies the mechanism in this process. After the test started, the sand particles near the downstream mudline began to oscillate periodically, probably due to the distribution pattern of the [...] Read more.
This paper visualizes the onset of scour under a pipeline in regular waves and studies the mechanism in this process. After the test started, the sand particles near the downstream mudline began to oscillate periodically, probably due to the distribution pattern of the seepage hydraulic gradient under the pipeline as well as asymmetric waves. As the wave height gradually increased, the sand under the pipeline began to oscillate at increasing amplitude and the coverage of oscillation extended upstream. Some sand rushed out from the bottom of the pipeline, and the sand oscillated almost symmetrically around the bottom line of the pipeline thereafter. The oscillation amplitude of the sand particles continued to rise, probably due to a decrease in the seepage path under the pipeline and loosened sediment in the oscillation. The scour onset occurred after more sand rushed out from under the pipeline. The visualization results reproduced the delay in the scour onset reported previously, and related the delay to the aforementioned increase in sediment oscillation amplitude. This visualization can improve the understanding of the scour onset mechanism, and can serve as a guide to further investigate the critical conditions of scour onset and scour control countermeasures for offshore structures. Full article
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